Official Series Description


Lab Data Summary

Aggregate lab data for the ARIKARA soil series. This aggregation is based on all pedons with a current taxon name of ARIKARA, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to ARIKARA were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
5478ND02500778ND025007Arikara6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6516667,-102.4988889
5478ND02500878ND025008Arikara6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6552778,-102.5208333
5406N0407S2005ND025002Arikara7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5495834,-102.8119965

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ARIKARA soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ARIKARA series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the ARIKARA series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ARIKARA series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with ARIKARA share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the ARIKARA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ARIKARA series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with ARIKARA, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. ND-2010-09-27-02 | Billings County - 2005

    Typical pattern of soils and underlying material in the Patent-Badland, outcrop-Cabbart association (Soil Survey of Billings County, North Dakota; 2005).

Map Units

Map units containing ARIKARA as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Badland-Arikara-Cabbart complex, 15 to 70 percent slopesL3191F4181027070622q1x9nd00719981:24000
Boxwell-Cabbart-Arikara complex, 9 to 70 percent slopesL2633F1703627070492q1xpnd00719981:24000
Lonna-Arikara-Cabbart complex, 9 to 70 percent slopesL2631F1013027070482qxknnd00719981:24000
Maltese-Lonna-Arikara complex, 2 to 50 percent slopesL2321F508927070452qxkdnd00719981:24000
Kirby-Arikara-Badland complex, 9 to 70 percent slopesL3104F439127070572q2mznd00719981:24000
Rhame-Arikara-Fleak complex, 9 to 70 percent slopesL1661F415427070402qxhwnd00719981:24000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F116226990621vztvnd00719981:24000
Shibah-Rubble land-Arikara complex, 15 to 70 percent slopesL4506F41727070822qxjsnd00719981:24000
Arikara-Cabbart loams, 15 to 70 percent slopesL3199F1027584402q1wynd00719981:24000
Badland-Arikara-Cabbart complex, 15 to 70 percent slopesL3191F11962027071252q1x9nd02519811:20000
Rhame-Arikara-Fleak complex, 9 to 70 percent slopesL1661F1479227071432qxhwnd02519811:20000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F991217146451vztvnd02519811:20000
Cabba-Badland-Arikara complex, 9 to 70 percent slopesE3103F785027072182qz6wnd02519811:20000
Arikara-Cabbart loams, 15 to 70 percent slopesL3199F368527071242q1wynd02519811:20000
Arikara-Cabba loams, 15 to 70 percent slopesE3199F11562707223d1y4nd02519811:20000
Zahl-Williams-Arikara loams, 9 to 45 percent slopesE3569F3952758488d1xznd02519811:20000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F12127584731vzt0nd02519811:20000
Boxwell-Cabbart-Arikara complex, 9 to 70 percent slopesL2633F2827584962q1xpnd02519811:20000
Zahl-Cabba-Arikara complex, 9 to 70 percent slopesE3607F122758489cvswnd02519811:20000
Badland-Arikara-Cabbart complex, 15 to 70 percent slopesL3191F354427597702q1x9nd03319851:24000
Arikara-Cabbart loams, 15 to 70 percent slopesL3199F18827597732q1wynd03319851:24000
Lonna-Arikara-Cabbart complex, 9 to 70 percent slopesL2631F15527597622qxknnd03319851:24000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F6127597411vztvnd03319851:24000
Boxwell-Cabbart-Arikara complex, 9 to 70 percent slopesL2633F2027597632q1xpnd03319851:24000
Shibah-Rubble land-Arikara complex, 15 to 70 percent slopesL4506F1327597772qxjsnd03319851:24000
Badland-Arikara-Cabbart complex, 15 to 70 percent slopesL3191F8019827151262q1x9nd05320031:24000
Boxwell-Cabbart-Arikara complex, 9 to 70 percent slopesL2633F3476827151292q1xpnd05320031:24000
Zahl-Cabba-Arikara complex, 9 to 70 percent slopesE3607F342622715120cvswnd05320031:24000
Rhame-Arikara-Fleak complex, 9 to 70 percent slopesL1661F1922627151452qxhwnd05320031:24000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F1843627150791vztvnd05320031:24000
Cabba-Badland-Arikara complex, 9 to 70 percent slopesE3103F907627150922qz6wnd05320031:24000
Maltese-Lonna-Arikara complex, 2 to 50 percent slopesL2321F364627151482qxkdnd05320031:24000
Kirby-Arikara-Badland complex, 9 to 70 percent slopesL3104F336227151352q2mznd05320031:24000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F309127150611vzt0nd05320031:24000
Arikara-Cabbart loams, 15 to 70 percent slopesL3199F232427151252q1wynd05320031:24000
Zahl-Williams-Arikara loams, 9 to 45 percent slopesE3569F23112715118d1xznd05320031:24000
Arikara-Cabba loams, 15 to 70 percent slopesE3199F5982715097d1y4nd05320031:24000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F806417183551vztvnd05919981:20000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F240717183471vzt0nd05919981:20000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F3389426625191vztvnd06119881:24000
Boxwell-Cabbart-Arikara complex, 9 to 70 percent slopesL2633F21727585342q1xpnd08719741:20000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F2356817135311vztvnd08919651:20000
Vebar-Arikara-Flasher complex, 9 to 50 percent slopesE1661F330317135051vzt0nd08919651:20000
Arikara-Cabba loams, 15 to 70 percent slopesE3199F702715998d1y4nd08919651:20000
Arikara-Shambo-Cabba loams, 9 to 70 percent slopesE2725F3126625681vztvnd10519931:24000

Map of Series Extent

Approximate geographic distribution of the ARIKARA soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .